A Persistent Deep Anticyclonic Vortex in the Rockall Trough Sustained by Anticyclonic Vortices Shed From the Slope Current and Wintertime Convection
| Type | Article | ||||||||||||||||
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| Date | 2020-10 | ||||||||||||||||
| Language | English | ||||||||||||||||
| Author(s) | Smilenova Angelina1, 2, Gula Jonathan3, Le Corre Mathieu3, Houpert Loïc4, Reecht Yves5 | ||||||||||||||||
| Affiliation(s) | 1 : Earth and Ocean Sciences, School of Natural Sciences, National University of Ireland, Galway (NUIG) University Road Galway ,Ireland 2 : Oceanographic Services, Marine Institute Galway ,Ireland 3 : University of Brest, CNRS, IRD, Ifremer, Laboratoire d'Océanographie Physique et Spatiale (LOPS), IUEM Brest, France 4 : National Oceanography Centre (NOC) Southampton, UK 5 : Institute of Marine Research Bergen, Norway |
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| Source | Journal Of Geophysical Research-oceans (2169-9275) (American Geophysical Union (AGU)), 2020-10 , Vol. 125 , N. 10 , P. e2019JC015905 (27p.) | ||||||||||||||||
| DOI | 10.1029/2019JC015905 | ||||||||||||||||
| WOS© Times Cited | 10 | ||||||||||||||||
| Keyword(s) | mesoscale eddy, eddy merger, instability, potential vorticity transformations, topographic effects, water masses mixing, Rockall Trough | ||||||||||||||||
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